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Precipitation Gravimetry01:03

Precipitation Gravimetry

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Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
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Measuring Acceleration Due to Gravity01:12

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Consider a coffee mug hanging on a hook in a pantry. If the mug gets knocked, it oscillates back and forth like a pendulum until the oscillations die out.
A simple pendulum can be described as a point mass and a string. Meanwhile, a physical pendulum is any object whose oscillations are similar to a simple pendulum, but cannot be modeled as a point mass on a string because its mass is distributed over a larger area. The behavior of a physical pendulum can be modeled using the principles of...
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Instrument Calibration01:12

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Instrument calibration is essential for ensuring that instruments produce accurate and consistent results. It is vital in manufacturing, healthcare, testing laboratories, and scientific research. Calibration processes are specific to each instrument and help enhance data accuracy. Each instrument has a unique calibration process tailored to its design and function to improve data accuracy.
Analytical Balance Calibration
An analytical balance measures mass and requires regular calibration to...
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Gravimetry: Overview01:05

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Gravimetric analysis is a quantitative method where the analyte is isolated and weighed directly or after conversion into a substance of known composition. Gravimetric analysis can be classified as precipitation, electrogravimetry, volatilization, and particulate gravimetry, based on the method used to isolate the analyte.
In precipitation gravimetry, the analyte is converted into a precipitate and weighed. For example, the silver content in a sample can be estimated by precipitating and...
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Uncertainty in Measurement: Accuracy and Precision03:37

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Scientists typically make repeated measurements of a quantity to ensure the quality of their findings and to evaluate both the precision and the accuracy of their results. Measurements are said to be precise if they yield very similar results when repeated in the same manner. A measurement is considered accurate if it yields a result that is very close to the true or the accepted value. Precise values agree with each other; accurate values agree with a true value. 
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Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

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During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance.
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Updated: Oct 8, 2025

Manufacturing Simple and Inexpensive Soil Surface Temperature and Gravimetric Water Content Sensors
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Improving Groundwater Model Calibration with Repeat Microgravity Measurements.

Jeffrey R Kennedy1, Libby Wildermuth2, Jacob E Knight2

  • 1U.S. Geological Survey, 2255 N Gemini Dr., Flagstaff, AZ, 86001.

Ground Water
|December 24, 2021
PubMed
Summary
This summary is machine-generated.

Repeat microgravity measurements offer a novel way to estimate groundwater parameters. This method, validated with MODFLOW and field data, improves estimates of hydraulic conductivity and specific yield by reducing uncertainty.

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Area of Science:

  • Hydrogeology
  • Geophysics

Background:

  • Groundwater-flow models traditionally rely on hydraulic head and flux data for calibration.
  • Parameter estimation in groundwater models is crucial for accurate water resource management.
  • Repeat microgravity measurements provide a novel type of observation for groundwater studies.

Purpose of the Study:

  • To demonstrate the utility of repeat microgravity data for groundwater model parameter estimation.
  • To integrate microgravity-derived changes in storage into groundwater model objective functions.
  • To evaluate the effectiveness of this method using field data and MODFLOW simulations.

Main Methods:

  • Simulating gravity changes from a MODFLOW groundwater model.
  • Incorporating microgravity observation misfits into the model's objective function.
  • Utilizing new software linked to MODFLOW input/output files and field data.

Main Results:

  • A 10-year microgravity survey near the All American Canal showed gravity decreases (up to 100 μGal) correlating with reduced seepage after canal lining.
  • Simulated gravity from a MODFLOW model closely matched the observed microgravity data.
  • Repeat microgravity data significantly reduced uncertainty in hydraulic conductivity and specific yield estimates compared to using only drawdown data.

Conclusions:

  • Repeat microgravity measurements are a valuable tool for estimating groundwater parameters, particularly specific yield and hydraulic conductivity.
  • The method effectively constrains model parameters by simulating gravity changes and including observation misfits.
  • The addition of microgravity data enhances the reliability of groundwater model predictions.